Karisimbi
Stratovulcano · DR Congo-Rwanda · 4490 m

- Tipo
- Stratovulcano
- Paese
- DR Congo-Rwanda
- Regione
- Eastern Africa Volcanic Regions / Albertine Rift Volcanic Province
- Altitudine
- 4490 m
- Coordinate
- -1.506, 29.450
- Ultima eruzione
- -8050
- Contesto tettonico
- Rift zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Trachybasalt / Tephrite Basanite
Sintesi geologica
Karisimbi is a complex basanitic-to-trachytic volcano with a symmetrical sharp-peaked summit. The 2-km-wide Branca caldera, located SE of the summit, is filled by viscous lava flows and two explosion craters. The large 1.2-km-wide Muntango pit crater is located south of the summit. A broad lava plain, formed from lava flows erupted within the caldera and along a chain of cones, extends SW. More than 100 cones erupted along a NNE-SSW zone that extends to the shores of Lake Kivu. The youngest Potassium-Argon date obtained is about 10,000 years before present (de Mulder, 1985). The youngest eruptions produced a group of dome-shaped vents east of the caldera, which fed viscous lava flows that traveled as far as 12 km E, and lava flows from the SW-flank lava vents.
Sintesi da Wikipedia
Il monte Karisimbi è un vulcano in fase di quiescenza nella catena dei Monti Virunga al confine tra Ruanda e Repubblica Democratica del Congo.
Wikipedia · CC BY-SA · Leggi l'articolo completo →
Storia delle eruzioni
Cronologia dettagliata
- 8050 a.C.VEI ?Stima geologicaBCE 8050 – In corso
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.